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921.
2011年6月14日至17日,国土资源部油气中心选区项目在上海召开了针对东海陆架盆地南部地区的中生界勘探新领域在地震资料解释和成盆地质方面的关键地质问题研讨会议。 相似文献
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924.
海三棱藨草Scirpus mariqueter是中国特有盐沼植物,也是长江口淤涨型潮滩的典型盐沼先锋植物。在自然状况下,盐沼植被依照盐渍藻类—海三棱藨草—芦苇进行演替。近10年来,由于受长江口的高强度围垦、外来入侵种互花米草的大面积引种和长江中上游来沙量的锐减及全球气候变暖引起的海平面上升的迭加效应影响,海三棱藨草的面积呈加速缩减态势,如若不及时采取相应的保护措施,海三棱藨草将面临灭种的威胁,并由此带来长江河口滩涂湿地生态系统结构和功能的改变。为此,需对长江口滩涂围垦、互花米草种植促淤的人为措施进行深入研究,以保护好中国特有的盐沼植物海三棱藨草,维持长江河口湿地生态系统结构和功能的完整性,更好地发挥其湿地生态系统的服务功能。 相似文献
925.
辽东半岛南部印支造山旋回早期的顺层滑脱构造 总被引:3,自引:0,他引:3
辽东半岛南部发育于太古宙基底与青白口系盖层邻接部位的大型韧性剪切带与盖层内顺层固态流变形成的构造群体,是印支造山旋回开始时,在主要来自太平洋方面的构造力驱动下,以盖层与基底的不整合面为主滑脱面发生自东向西近水平多层系顺层剪切滑脱的产物, 称顺层滑脱构造。大范围的顺层滑脱未引起大规模的褶皱—逆冲推覆;同时,主滑脱面也不同于伸展拆离断层。顺层滑脱构造形成后先后被南北向(T3 —J1) 和东西向(J2 —J3) 等褶皱断裂系叠加改造;基底在晚白垩世的断块运动中大幅度抬升。顺层滑脱构造应该是长期沉降的沉积盆地在进入造山旋回时( 主褶皱前) 可能出现的构造型式。 相似文献
926.
基于遥感资料的陕北黄土高原植被覆盖率时空特征分析 总被引:1,自引:0,他引:1
选取黄土高原的典型区域--陕北作为监测区域,以MODIS和TM资料作为主要数据源,从可业务化的角度采用植被指数法进行了植被覆盖率的遥感反演,对4种生态气候区植被覆盖率季相变化特征进行了分析,并对陕北生态环境治理前后植被覆盖率的变化进行了对比,结果表明:生态治理后陕北黄土高原的植被覆盖率绝大多数地区都是正增长,各生态气候区植被覆盖状况都有了不同程度的改善,生态治理效果最明显的区域在陕北南部. 相似文献
927.
The circulations off the Changjiang mouth in May and November were simulatedby a three dimension numerical model with monthly averaged parameters of dynamic factors in this paper. The area covers the East China Sea (ECS), Yellow Sea and Bohai Sea. Simulated results show that the circulation off the Changjiang mouth in spring and autumn is mainly the Changjiang runoff and Taiwan Warm Current (TWC). The Changjlang discharge is much larger in May than in November, and the wind is westward in May, and southward in November offthe Changjiang mouth. The runoff in May branches in three parts, one eastward flows, the other two flow northward and southward along the Subei and Zhejiang coast respectively. The Changjiang diluted water expands eastward off the mouth, and forms a strong salinity front near the mouth. Surface circulation in autumn is similar to that in winter, the runoff southward flows along the coast, and the northward flowing TWC becomes weaker compared to that in spring and summer. The bottom circulations in May and November are mainly the runoff near the mouth and the TWC off the mouth, and the runoff and TWC are greater in May than in November. 相似文献
928.
Based on the temperature data along 34°N, 35°N and 36°N sections in August from 1977 to 2003, the structure and formation of the Southern Yellow Sea Cold Water Mass (SYSCWM) and its responses to El Nino events are analyzed. Results show that: (1) There exist double cold cores under the main thermocline along the 35°N and 36°N sections. Also, double warm cores exist above the main thermocline along the 36°N section. (2) Thermocline dome by upwelling separates the upper warm water into two parts, the eastern and western warm waters. Additionally, the circulation structure caused by upwelling along the cold front and northeastward current along the coast in summer is the main reasons of double warm cores along the 36°N section. The intermediate cold water is formed in early spring and moves eastward slowly, which results in the formation of the western one of double cold cores. (3) Position of the thermocline dome and its intensity vary interannually, which is related to El Nino events. However, the 相似文献
929.
Suspended sediment load in the turbidity maximum zone at the Yangtze River Estuary:The trends and causes简 总被引:6,自引:2,他引:4
Based on the analysis of suspended sediment elements at estuaries, influence of human activities and estuarine regulation projects on the turbidity maximum zone was studied according to the measurement data between 1959 and 2011. It was found that human activi- ties had little effect on the seaward water while the sharp decrease of sediment volume and concentration in runoff led to the sharp decrease of turbidity maximum zone in the estuary. The concentration at outside sea and Hangzhou Bay did not change, and that along the Subei coast also decreased a little, which had no influence on the turbidity maximum zone. Com- pared with the concentration between 1959 and 1999, the peak of concentration moved up- stream in the estuary, and the concentration in 2000-2009 decreased by about 24.73% with a narrower variation range along the river to the sea. The suspended sediment concentration in North Passage was low in upstream and downstream because of the decrease of seaward sediment and coarsening of bed material, while it was relatively high in the middle due to the influence of sediment cross the north jetty. 相似文献
930.